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Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation

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Presentation on theme: "Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation"— Presentation transcript:

1 Charlotte-Rock Hill-Gastonia MSA Summertime Ozone Formation
Photos from 2001 Mecklenburg Country State of the Environment Report

2 Arizona’s Valley of the Sun “Brown Cloud”
Phoenix photo from accessed Mar 2004 Observed since early 1990’s; contains C Particles and NO2 (brown) gas From burning fossil fuels: cars, construction equipment, power plants, lawn mowers, leaf blowers contribute to this brown cloud Weather also a key factor

3 Image take from http://www. al. noaa. gov/WWWHD/Pubdocs/TropoRural
Image take from accessed Mar 2004

4 Presence of NO2 (brown gas) results in inevitable formation of ozone
NO2 (brown) + sunlite  NO• + O• O• + O2  O3 (Ozone) Control measures to effectively address ground-level ozone must focus on minimizing NO2 formation

5 Ozone precursors Nitrogen Oxides
Dry Air is 78% Nitrogen (N2), 21% Oxygen (O2) Heating air to high temperatures forms NO• (motor vehicles, fossil-fuel power plants, lightning) NO• is an ozone precursor and also reacts directly with ozone to destroy it Volatile Organic Compounds (VOC’s) VOC’s continuously emitted by fuel spills, motor vehicles, trees, air fresheners, paints, and countless other sources OH• hydroxyl radical is the atmosphere’s “natural detergent” that cleans VOC’s from the air by initiating the process that converts them into carbon dioxide and water

6 Volatile Organic Compound (VOC) Removal
Air’s natural VOC cleanser produced from ozone and water Ozone (O3) + UV-B -> O2+ *O• *O• + H2O  2OH• OH• works by transforming stable VOC molecules (R-H) into reactive radicals (R•) OH• + R-H  R• + H2O Reactive organic radicals immediately combine with oxygen to form peroxide radicals R• + O2  (R-O-O•)

7 Formation of Nitrogen Dioxide
NO• + R-O-O•  NO2• + RO• Formation of NO2 (and O3) driven primarily by: Concentration of VOC’s (near emission sources) Concentration of NO• (rural & downwind areas) Concentrations of both NO• and VOC’s ***Summertime ozone pollution results from an overload in our air of NO•, VOC’s, or both

8 NO and VOC Effects on Ozone Production
Both NO• + VOC Sensitive VOC Sensitive Region NO• Sensitive Region Both NO• + VOC Sensitive Figure from : accessed Mar 2004

9 ’95-’99 AM NMOC/NOy Ratios for the Plaza Monitoring Site
20 NO Limited x 15 y NMOC/NO 10 VOC Limited 5 1994 1995 1996 1997 1998 1999 2000 From Perry, JL and Owens, PM, “Weekday/Weekend Variability and Long-Term Trends in Traffic, CO, NOy, and Ozone for the Charlotte Metropolitan Area during the 1990's, AWMA, June 2001

10 I-77 Traffic Volume vs. Time of Day
5000 4000 3000 Hourly Volume 2000 1000 Time of Day (Hour) Sun Mon Tues Wed Thu Fri Sat From Perry and Owens, AWMA, 2001

11 May-Sep ‘95-‘98 Plaza Average Hourly NOy
40 y 35 30 25 Avg Hourly NO Concentration (ppb) 20 15 10 5 1 3 5 7 9 11 13 15 17 19 21 23 Time of Day Sunday Monday Tuesday Wednesday Thursday Friday Saturday From Perry and Owens, AWMA, 2001

12 1990-1998 May-Sep Diurnal Charlotte Ozone Averages
By Day of Week (weekend days-lines, weekdays-markers From Perry and Owens, AWMA, 2001

13 Obtained from John White, NC DAQ

14 From: http://www. epa. gov/airnow/showmaps. html
From: accessed Mar 2004

15 From: http://www. epa. gov/airnow/showmaps. html
From: accessed Mar 2004


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